2026-05-16T08:34:48Zhttp://doidb.wdc-terra.org/oaip/oaioai:doidb.wdc-terra.org:8652016-11-25T15:11:04ZDOIDBDOIDB.SDDBfalse3DOIDB.SDDB
10.1594/GFZ.SDDB.1046
Rioual, Patrick
Mackay, Anson
Age models based on palaeomagnetic measurements for the two cores analysed, CON01-603-2 (Continent Ridge) and VER98-1-14 (Academician Ridge) showing the correlation points to the reference record
Deutsches GeoForschungsZentrum GFZ
2006
Vereshchagin 98 Expedition
Vereshchagin Long Cores Expedition 2001
R/V Vereshchagin
age (calendar years)
correlation of paleointensity records
2006-09-15
eng
Dataset
10.1016/j.gloplacha.2004.08.002
15 Datapoints
text/tab-separated-values
Palaeomagnetism was the method used for dating sediments older than the time span covered by AMS 14C dating. Geomagnetic palaeointensities recorded in Lake Baikal sediments were tuned to a reference curve (the record from ODP Site 984, Channell, 1999) whose chronology is well constrained (Demory et al., 2005a-this volume and Demory et al., 2005b-this volume). The palaeointensity record from ODP Site 984 is of high quality, is well dated and covers the time span of the present study. Anchored by a geomagnetic excursion (the Iceland basin event, dated at 186–189 ka according to Channell et al. (1997)), this age model is constrained by 55 correlation points for a time span of ca. 200 ky. The age models for both core sections in the interval 100–150 ky are shown in Fig. 2.
53.523 107.9694 53.9632 108.9139